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Composite transite

S. No. Transition metal-rare earth metal composition Transition metal (mg/l) Rare earth metal (mg/l) Transition metal Rare earth metal... [Pg.297]

The equations presented in this section are equivalent to drawing straight lines to show the gas composition transitions. The equations are frequently easier to use and provide a more precise result than manually drawn lines. [Pg.576]

Figure 6.21. A scheme of a frequent pathway following ancient gene duplications blue bars). One copy is supposed to be preferentially transposed into the ancestral genome core (pint bar) which then undergoes the major compositional transition (red bars). (From Jabbari ct al.. 200. b). Figure 6.21. A scheme of a frequent pathway following ancient gene duplications blue bars). One copy is supposed to be preferentially transposed into the ancestral genome core (pint bar) which then undergoes the major compositional transition (red bars). (From Jabbari ct al.. 200. b).
Figure 11.1. A schematic representation of A the major , B the minor , and C the whole-genome , or horizontal , compositional transitions, or shifts, in the genomes of vertebrates. This scheme displays the CsCI profiles (which are good approximations of the compositional distributions of DNA molecules) along with the changes that follow the compositional shift under consideration (broken lines). A refers to the transitions between cold- and warm-blooded vertebrates B to the transition between the general mammalian pattern and the murid pattern C to the transitions among cold-blooded vertebrates D to the conservative mode of evolution. (Modified from Bernardi et al., 1997). Figure 11.1. A schematic representation of A the major , B the minor , and C the whole-genome , or horizontal , compositional transitions, or shifts, in the genomes of vertebrates. This scheme displays the CsCI profiles (which are good approximations of the compositional distributions of DNA molecules) along with the changes that follow the compositional shift under consideration (broken lines). A refers to the transitions between cold- and warm-blooded vertebrates B to the transition between the general mammalian pattern and the murid pattern C to the transitions among cold-blooded vertebrates D to the conservative mode of evolution. (Modified from Bernardi et al., 1997).
These findings indicate that the compositional transitions affecting the genome core of... [Pg.308]

The compositional differences that were found among species belonging to different orders and to different families within the same order are indicative of whole genome, or horizontal, compositional transitions. These transitions were found to be independent of geological time (see Fig. 11.18). Moreover, the rates of directional base substitutions responsible for the transitions were found to be very variable and to reach, in some cases, extremely high values (Bernardi and Bernardi, 1990b). [Pg.323]

Undoubtedly, the simplest explanation for the striking similarity of mammalian/avian data would be that this similarity is the consequence of a compositional transition in the common ancestor of mammals and birds. The ancient Haematotherma hypothesis (Haeckel, 1866 Owen, 1866 a hypothesis revived by Hedges et al., 1990), which puts mammals and birds in sister groups, whose common ancestor might have undergone the transition would have satisfied this requirement, if the hypothesis had not been disposed of (see Caspers et al., 1996, and Janke et al., 2001, for discussions on this point). [Pg.356]

The independent compositional transitions that occurred in the ancestral lines of mammals and birds were accompanied by other functionally important changes 1) CpG and... [Pg.379]

Bernardi G. and Bernardi G. (1990b). Compositional transitions in the nuclear genomes of cold-blooded vertebrates. J. Mol. Evol. 31 282-293. [Pg.395]

Bernardi G., Hughes S., Mouchiroud D. (1997). The major compositional transitions in the vertebrate genome a review. J. Mol. Evol. 44 S41-S51. [Pg.396]

Cruveiller S., D Onofrio G., Bernard G. (2000). The compositional transition between the genomes of cold- and warm-blooded vertebrates codon frequencies in orthologous genes. Gene 261 71-83. [Pg.401]

Final State Composition Transition Energy (eV) Oscillator Strength ... [Pg.318]

Fig. 6.3. Numerical modeling of the thermal regime in the lithosphere of the Oued el-Mya Basin, Takhoukht region. Solid line ist the base of the lithosphere as determined by intersection of the current geotherm with solidus curve for peridotite (shown in Fig. 6.4). Long dashed lines are isotherms Moho = base of the crust comp, transition = location of pyroxene peridotite-garnet peridotite compositional transition in the mantle. The considerable rise of isotherms is related to periods of thermal activation in the lithosphere in the Permian-Tfiassic and Cretaceous, Reduction of the crust thickness occurred during basement stretching (in the Ordovician-Devonian and Cretaceous) and during Permian erosion... Fig. 6.3. Numerical modeling of the thermal regime in the lithosphere of the Oued el-Mya Basin, Takhoukht region. Solid line ist the base of the lithosphere as determined by intersection of the current geotherm with solidus curve for peridotite (shown in Fig. 6.4). Long dashed lines are isotherms Moho = base of the crust comp, transition = location of pyroxene peridotite-garnet peridotite compositional transition in the mantle. The considerable rise of isotherms is related to periods of thermal activation in the lithosphere in the Permian-Tfiassic and Cretaceous, Reduction of the crust thickness occurred during basement stretching (in the Ordovician-Devonian and Cretaceous) and during Permian erosion...

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See also in sourсe #XX -- [ Pg.298 ]




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